Fluid evolution of the Qiman Tagh W-Sn ore belt, East Kunlun Orogen, NW China
Abstract
The Qiman Tagh W-Sn ore belt is located in the westernmost sector of the East Kunlun Orogen, NW China. It has been recognized as a unique W-Sn belt that formed in the early Paleozoic and related to closure of the Proto-Tethys. To understand the evolution of ore-forming fluids and its relationship with the tectonic setting of East Kunlun Orogen, we report the results obtained from fluid inclusion and H-O isotopic studies of ores and quartz veins...
Paper Details
Title
Fluid evolution of the Qiman Tagh W-Sn ore belt, East Kunlun Orogen, NW China
Published Date
Apr 1, 2018
Journal
Volume
95
Pages
280 - 291
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